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The composite Kaçkar batholith, of Cretaceous to Late Eocene age, consists of various intrusions derived from different geodynamic settings ranging from early to mature arc, through collision, to post-collisional extension in the Neo-Tethyan convergence system of the eastern Pontides of NE Turkey. The intrusions were emplaced into Cretaceous and Middle Eocene volcano-sedimentary units, and are unconformably...